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Pressurized Water Reactor (PWR) Models: Involve neutron transport, thermal-hydraulics, chemistry Inherently multi-scale, multi-physics CRUD Measurements: Consist of low resolution images at limited number of locations.

Pressurized Water Reactor (PWR)Pressurized Water Reactor (PWR) Models: • Involve neutron transport, thermal-hydraulics, chemistry • Inherently multi-scale, multi-physics CRUD Measurements:

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  • Pressurized Water Reactor (PWR)

    Models:

    •  Involve neutron transport, thermal-hydraulics, chemistry

    •  Inherently multi-scale, multi-physics CRUD Measurements: Consist of low resolution images at limited number of locations.

  • Pressurized Water Reactor (PWR)

    3-D Neutron Transport Equations:

    Challenges:

    •  Linear in the state but function of 7 independent variables:

    •  Very large number of inputs or parameters; e.g., 100,000; Parameter selection critical.

    •  ORNL Code: Denovo •  Codes can take hours to days to run.

  • Pressurized Water Reactor (PWR) Thermo-Hydraulic Model: Mass, momentum and energy balance for fluid

    Challenges:

    •  Nonlinear coupled PDE with nonphysical parameters due to closure relations;

    •  CASL code: COBRA (CTF) •  COBRA is a sub-channel code, which cannot be resolved between pins. •  Codes can take minutes to days to run.

    Note: Similar equations for gas

  • Microscopic Cross-Sections

    Cross-Sections: Probability that a neutron-nuclei reaction will occur is characterized by nuclear cross-sections.

    •  Assume target is sufficiently thin so no shielding. •  Rate of Reactions:

    •  Microscopic Cross-Sections: Related to types of reactions.

    Flux I

    NA

    neutrons

    cm

    2 · s

    nuclei

    cm2R = �INA

    Note: � is microscopic cross-section (cm2)

    �f : Fission

    �s: Scatter�t: Total

    Reference: J.J. Duderstadt and L.J. Hamilton, Nuclear Reactor Analysis, John Wiley and Sons, 1976.

  • Macroscopic Cross-Sections

    Macroscopic Cross-Sections: Accounts for shielding

    Total Reaction Rate per Unit Area:

    dR = �tIdNA

    = �tINdx

    Strategy: Equate reaction rate to decrease in intensity

    �dI(x) = �[I(x+ dx)� I(x)]= �tINdx

    ) dIdx

    = �N�tI(x)

    ) I(x) = I0e�N�tx

    Total Macroscopic Cross-Section: ⌃t ⌘ N�tFrequency: With which reactions occur v⌃t

    cm

    s

    1

    cm=

    1

    s

    I0

  • Neutron Flux in Reactor

    Neutron Density: N(r, t)

    • N(r, t)dr3: Expected number of neutrons in dr3 about r at time t

    Reaction Rate Density: Interaction frequency

    dr3

    r

    • N(r, E, t)dr3dE: Expected number neutrons in dr3 with energies E in dE

    Angular Neutron Density:

    • n(r, E, ⌦̂, t)dr3dEd⌦̂: Expected number of neutrons in dr3 about rwith energy E about dE, moving in direction ⌦̂

    in solid angle ⌦̂ at time t

    Angular Neutron Flux: '(r, E, ⌦̂, t) = vn(r, E, ⌦̂, t)

    F (r, E, t)dr3 = v⌃N(r, E, t)dEdr3

    v⌃ where v is neutron speed

  • Neutron Transport Equation Conservation Law:

    Gain Mechanisms: (1) Neutron sources (fission)

    (2) Neutrons entering V

    (3) Neutrons of different E0, ⌦̂0 that change to E, ⌦̂ due to scattering collision

    Loss Mechanisms: (4) Neutrons leaving V

    (5) Neutrons suffering a collision

    @

    @t

    Z

    Vn(r, E, ˆ⌦, t)dr3

    �= gain in V � loss in V

  • Neutron Transport Equation Terms:

    (1)

    Z

    VS(r, E, ⌦̂, t)dr3dEd⌦̂ where S is a source term

    (5) Rate at which neutrons collide at point r is

    ) (5) =hR

    V vP

    t(r, E)n(r, E, ⌦̂, t)dr3idEd⌦̂

    j(r, E, ⌦̂, t) · dS = v⌦̂n(r, E, ⌦̂, t) · dSso leakage is

    =

    Z

    Vr · v⌦̂n(r, E, ⌦̂, t)dr3

    �dEd⌦̂

    =

    Z

    Vv⌦̂ ·rn(r, E, ⌦̂, t)dr3

    �dEd⌦̂

    (2), (4) Consider the rate at which neutrons leak out of surface

    (4) - (2) =

    Z

    SdS · v⌦̂n(r, E, ⌦̂, t)

    �dEd⌦̂

    ft = v⌃t(r, E)n(r, E, ⌦̂, t)

  • Neutron Transport Equation Terms: Scattering cross-sections

    •  Consider first a beam of neutrons of incident intensity I, all of energy E’, hitting a thin target of surface atomic density NA

    E0 E

    Note: Microscopic differential scattering cross-section is proportionality constant

    Rate

    cm2= �s(E

    0 ! E)INAdE

    Microscopic scattering cross-section:

    �s(E0) =

    Z 1

    0dE�s(E

    0 ! E)

    when neutron scatters from energy E0 to final energy E in range E to E+dE

    Macroscopic scattering cross-section:

    ⌃s(E0 ! E) ⌘ N�s(E0 ! E)

  • Neutron Transport Equation Terms: Scattering cross-sections

    •  Consider how change in direction

    ⌦̂0 ⌦̂�s(⌦̂

    0) =

    Z

    4⇡d⌦̂�s(⌦̂

    0 ! ⌦̂)

    (3) Rate at which neutrons scatter from E0, ⌦̂0 to E, ⌦̂ isZ

    Vv0⌃s(E

    0 ! E, ⌦̂0 ! ⌦̂)n(r, E0, ⌦̂0, t)dr3�dEd⌦̂

    To incorporate contributions from any E0, ⌦̂0, we integrate to obtain

    (3) =

    Z

    Vdr3

    Z

    4⇡d⌦̂0

    Z 1

    0dE0v0⌃s(E

    0 ! E, ⌦̂0 ! ⌦̂)n(r, E0, ⌦̂0, t)�dEd⌦̂

  • Neutron Transport Equation Conservation Law:

    Since this must hold for any control volume, it follows that @n

    @t+ v⌦̂ ·rn+ v⌃tn(r, E, ⌦̂, t)

    0 =

    Z

    V

    @n

    @t+ v⌦̂ ·rn+ v⌃tn(r, E, ⌦̂, t)

    Angular Flux: '(r, E, ⌦̂, t) = vn(r, E, !̂, t)

    1

    v

    @'

    @t+ ⌦̂ ·r'+ ⌃t(r, E)'(r, E, ⌦̂, t)

    �Z 1

    0dE0

    Z

    4⇡d⌦̂0v0⌃s(E

    0 ! E, ⌦̂0 ! ⌦̂)n(r, E0, ⌦̂0, t)�S(r, E, ⌦̂, t)�dr3dEd⌦̂

    =

    Z

    4⇡d⌦̂0

    Z 1

    0dE0⌃s(E

    0 ! E, ⌦̂0 ! ⌦̂)'(r, E0, ⌦̂0, t) + S(r, E, ⌦̂, t)

    =

    Z

    4⇡d⌦̂0

    Z 1

    0dE0v0⌃s(E

    0 ! E, ⌦̂0 ! ⌦̂)n(r, E0, ⌦̂0, t) + S(r, E, ⌦̂, t)

  • Neutron Transport Equation Plane Symmetry: Flux depends only on x

    x

    ⌦̂

    ✓ = cos�1 µ• ⌦x

    = cos ✓

    •Z

    4⇡d⌦̂0 =

    Z ⇡

    0d✓0 sin ✓0

    Then ˆ

    ⌦ ·r' = ⌦x

    @'

    @x

    = cos ✓

    @'

    @x

    so 1

    v

    @'

    @t

    + cos ✓

    @'

    @x

    + ⌃t'(x,E, ✓, t)

    =

    Z ⇡

    0d✓

    0 sin ✓0Z 1

    0dE

    0⌃s(E0 ! E, ✓0 ! ✓)'(x,E0, ✓0, t) + S(x,E, ✓, t)

    1-D Neutron Transport Equation: 1

    v

    @'

    @t

    + µ@'

    @x

    + ⌃t'(x,E, µ, t)

    =

    Z 1

    �1dµ

    0Z 1

    0dE

    0⌃s(E0 ! E, µ0 ! µ)'(x,E0, µ0, t) + S(x,E, µ, t)